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dc.contributor.advisorSawyer, Audrey
dc.creatorMadson, Michael
dc.date.accessioned2019-05-01T00:50:53Z
dc.date.available2019-05-01T00:50:53Z
dc.date.issued2019-05
dc.identifier.urihttp://hdl.handle.net/1811/87608
dc.description.abstractLimestone aquifers are important sources of drinking water in many regions of the United States, including Ohio. Here, I characterize properties of a limestone aquifer using data from an observation well that was installed as part of the Mirror Lake Water Science Learning Lab on The Ohio State University campus in Columbus, Ohio. I integrate drilling observations, a gamma ray log, and borehole camera footage to identify geologic formations and conductive features within the limestone. I also analyze slug test and pump test results to determine aquifer hydraulic conductivity. I show that the hydraulic conductivity is comparable with other local measurements and within the range of many limestone aquifers from other regions. I present three months of water level, temperature, and specific conductivity data from the observation well to explore the factors that influence water level and water quality in the limestone aquifer.en_US
dc.description.sponsorshipNSF EAR 1752995en_US
dc.language.isoen_USen_US
dc.publisherThe Ohio State Universityen_US
dc.relation.ispartofseriesThe Ohio State University. School of Earth Sciences Senior Theses; 2019en_US
dc.subjectMirror Lakeen_US
dc.subjectHydrogeologyen_US
dc.subjectHydraulic Conductivityen_US
dc.subjectmonitoring wellen_US
dc.titleAnalysis of Hydrogeologic Data from an Observation Well at Mirror Lake (Columbus, Ohio)en_US
dc.typeThesisen_US
dc.description.embargoNo embargoen_US


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